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Published on: August 17, 2016
Controls on blowout evolution in southern Portugal: A 49-year analysis
Lara Talavera1, Susana Costas2, Óscar Ferreira2
1Department of Biology, Geology, Physics and Inorganic Chemistry, School of Experimental Sciences and Technology (ESCET), Rey Juan Carlos University, C/Tulipán s/n, Móstoles, 28933 Madrid, Spain; Centre for Marine and Environmental Research (CIMA), Building 7, Faculty of Science and Technology, Gambelas Campus, University of Algarve, 8005-139 Faro, Portugal.
Coastal dune blowouts form through wind erosion, with genesis taking 1-2 years. Their full natural cycle likely exceeds five decades, influenced by complex ecogeomorphic feedbacks. Dune management should allow natural evolution.
Area of Science:
- Coastal geomorphology
- Dune dynamics
- Ecogeomorphology
Background:
- Blowouts are wind-formed depressions crucial for coastal dune sediment budgets and biodiversity.
- The drivers and temporal scales of blowout genesis, development, and decay are not well understood.
Purpose of the Study:
- To analyze the morphometric changes of blowouts over time.
- To identify the drivers and temporal scales of blowout evolution phases.
- To inform dune management strategies.
Main Methods:
- Digitized morphometric characteristics of blowouts from 1972-2021 imagery.
- Analyzed changes in blowout number, area, and shape over time.
- Correlated morphometric data with metocean and human activity time series.
Main Results:
- Blowout genesis phase (1-2 years) driven by physical factors and dune irregularities.
- Ongoing development phase shows expansion and rotation influenced by wind and internal factors.
- Natural decay phases were not observed; artificial sealing lasted 4 years.
- Reactivation occurred due to storm impacts on sealed blowouts.
Conclusions:
- A complete natural blowout cycle may exceed 50 years, driven by complex ecogeomorphic feedbacks.
- Natural evolution, rather than artificial sealing, is recommended for dune management.
- Storms can reactivate artificially stabilized blowouts.
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